USGS - science for a changing world

Mineral Resources On-Line Spatial Data

Mineral Resources > Online Spatial Data > Geology > by state > Vermont

Underhill Formation, Jay Peak Member

Underhill Formation, Jay Peak Member - Pale, silver-green, quartz-sericite-chlorite-albite schist, locally quartzitic. (Northern and Central Vermont).
StateVermont
NameUnderhill Formation, Jay Peak Member
Geologic ageCambrian
Original map labelCuj
CommentsPart of Green Mountains, Camels Hump Group The Underhill lies stratigraphically above basement rocks of Mount Holly Complex of Grenville (1 b.y.) age. Age changed to Late Proterozoic and(or) Early Cambrian (Slack and others, 1988) per VT020.
Primary rock typemica schist
Secondary rock typequartzite
Other rock types
Lithologic constituents
Major
Metamorphic > SchistPale, silver-green, quartz-sericite-chlorite-albite schist, locally quartzitic.
Incidental
Metamorphic > Metasedimentary > Metaclastic > QuartzitePale, silver-green, quartz-sericite-chlorite-albite schist, locally quartzitic.
Map references
Nicholson, S.W., Dicken, C.L., Horton, J.D., Foose, M.P., Mueller, J.A.L., and Hon, Rudi, 2006, Preliminary integrated geologic map databases for the United States: Connecticut, Maine, Massachusetts, New Hampshire, New Jersey, Rhode Island, and Vermont: U.S. Geological Survey Open-File Report 2006-1272.
Unit references
Doll, C.G., Cady, W.M., Thompson, J.B., Jr., and Billings, M.P., 1961, Centennial Geologic Map of Vermont: Vermont Geological Survey, Miscellaneous Map MISCMAP-01, scale 1:250,000.
Slack, J.F., Atelsek, P.H. and Grosz, A.E., 1988, Geology and geochemical survey of the Bristol Cliffs Wilderness, Addison County, Vermont: U.S. Geological Survey Miscellaneous Field Studies Map, MF-1593-A, 1 sheet, scale 1:24,000.
Geographic coverageOrleans

Show this information as [XML]

AccessibilityFOIAPrivacyPolicies and Notices

Take Pride in America logoUSA.gov logoU.S. Department of the Interior | U.S. Geological Survey
URL: http://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=VTCAuj;0
Page Contact Information: Peter Schweitzer